首页> 外文期刊>International Journal of Greenhouse Gas Control >Relocation of microseismicity using reflected waves from single-well, three-component array observations: Application to CO2 injection at the Aneth oil field
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Relocation of microseismicity using reflected waves from single-well, three-component array observations: Application to CO2 injection at the Aneth oil field

机译:使用单井,三组分阵列观测的反射波将微震性重新定位:在Aneth油田的二氧化碳注入中的应用

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摘要

Passive microseismic measurement is an important tool for monitoring underground behavior during CO2 geosequestration; such monitoring is necessary for maintaining maximum long-term safety. It is however difficult to deploy an ideal observation network at reasonable cost for obtaining reliable source locations. In this paper, we show the re-analysis results of microseismicity detected on a single vertical borehole array deployed at the Aneth oil field, where CO2 injection was conducted for enhanced oil recovery operation. The objective of the re-analysis was to obtain improved source depth estimates. We first show possible translation of microseismic source locations from preliminary results based on detailed waveform observations and ray-path modeling using a 7-layer velocity model. Then, a source location method using multiple reflection waves and the relative source location method for many small slave events is proposed, and modified source location results are compared with those obtained by the standard location method. From the modified source depth distribution, we can infer that most of the microseismic events likely occurred as a result of injection salt water disposal and not by CO2 injection at the Aneth field. In general, the proposed analytical technique provides a more reliable understanding of underground changes during CO2 injection by improving the depth accuracy of microseismic activity
机译:被动微震测量是监测二氧化碳地质封存过程中地下行为的重要工具。这样的监视对于维持最大的长期安全性是必要的。但是,难以以合理的成本部署理想的观测网络以获得可靠的震源位置。在本文中,我们显示了在Aneth油田部署的单个垂直井眼阵列上检测到的微地震的重新分析结果,在该油田中进行了二氧化碳注入以提高采油率。重新分析的目的是获得改进的源深度估计。我们首先显示基于详细的波形观测和使用7层速度模型的射线路径建模的初步结果,从初步结果可能得出的微震源位置的转换。然后,提出了使用多次反射波的源定位方法和许多小奴隶事件的相对源定位方法,并将修改后的源定位结果与标准定位方法获得的结果进行比较。从修改后的震源深度分布中,我们可以推断出,大多数微地震事件可能是由于注入盐水处理而不是由于Aneth油田的CO2注入而发生的。通常,通过提高微地震活动的深度精度,所提出的分析技术可以更可靠地了解注入二氧化碳的地下变化

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